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  • 2005-2009  (7)
  • 1975-1979  (3)
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  • 1
    Online-Ressource
    Online-Ressource
    San Diego :Elsevier Science & Technology,
    Schlagwort(e): Uranium-thorium dating. ; Electronic books.
    Materialart: Online-Ressource
    Seiten: 1 online resource (471 pages)
    Ausgabe: 1st ed.
    ISBN: 9780080564883
    Serie: Issn Series ; v.Volume 13
    DDC: 546.431
    Sprache: Englisch
    Anmerkung: Front Cover -- U-Th Series Nuclides in Aquatic Systems -- Copyright page -- Dedication to Karl K. Turekian -- Contents -- Contributors -- Chapter 1. Introduction -- 1. Overview -- 2. Organization of the Volume -- Acknowledgements -- References -- Chapter 2. U- and Th-Series Nuclides in the Atmosphere: Supply, Exchange, Scavenging, and Applications to Aquatic Processes -- 1. Introduction -- 2. Sources of U- and Th-Series Nuclides to the Atmosphere -- 3. Atmospheric Distributions -- 4. Aerosol Scavenging Residence Times Using 222Rn and its Daughters -- 5. Applications of Rn Daughters of Atmospheric Origin to Study Aquatic Processes -- 6. Processes across Aquatic Interfaces -- 7. Perspectives and Future Directions -- Acknowledgements -- References -- Chapter 3. U-Series Geochemistry in Weathering Profiles, River Waters and Lakes -- 1. Introduction -- 2. Radionuclide Fractionation in Surface Environments -- 3. Radioactive Disequilibria in Weathering Profiles and Soils -- 4. U Series in Rivers -- 5. Review of Models for U-Series Fractionation in Surficial Environments -- 6. U-Series Disequilibria in Lakes -- 7. Future Perspectives -- Acknowledgments -- References -- Chapter 4. Investigating Groundwater Processes Using U- and Th-Series Nuclides -- 1. Introduction -- 2. General Element Behavior in Groundwaters -- 3. Modeling Nuclide Transport in Aquifers -- 4. Obtaining Solutions to the Model Equations -- 5. Radon and Recoil Rates -- 6. Ra Isotopes -- 7. Th Isotopes -- 8. U Isotopes -- 9. 210Pb -- 10. Summary and Future Studies -- Acknowledgments -- References -- Chapter 5. Uranium- and Thorium-Series Nuclides as Tracers of Submarine Groundwater Discharge -- 1. Introduction -- 2. How U-Th Isotopes are Used to Quantify Submarine Groundwater Discharge (SGD) -- 3. Radium -- 4. Radon -- 5. Uranium -- 6. Synthesis of Existing Studies. , 7. Towards a Global Estimate of SGD -- 8. Perspectives and Future Directions -- Acknowledgments -- References -- Chapter 6. U- and Th-Series Nuclides in Estuarine Environments -- 1. Introduction: Estuarine Processes -- 2. Uranium -- 3. Thorium -- 4. Radium -- 5. Radon -- 6. Lead-210 and Polonium-210 -- 7. Future Studies -- References -- Chapter 7. U- and Th-Series Nuclides as Tracers of Particle Dynamics, Scavenging and Biogeochemical Cycles in the Oceans -- 1. Abundance and Distribution of U-Th Nuclides in the Sea -- 2. Introduction to Particle Cycling and Scavenging in the Ocean -- 3. The Scavenging Process as Understood from Thorium Isotopes -- 4. Scavenging and Th Speciation -- 5. 226Ra-210Pb-210Po -- 6. The Role of Particle Composition -- 7. Boundary Scavenging -- 8. Calibration of Vertical Particle Fluxes -- 9. Summary and Outlook -- References -- Chapter 8. The Bioaccumulation of U- and Th-Series Radionuclides in Marine Organisms -- 1. Introduction -- 2. Radionuclides of Interest and their Bioavailability -- 3. Models of Uptake and Trophic Transfer -- 4. Biodetritus and Vertical Transport -- 5. Potential Impacts of Natural Radioactivity -- 6. Synthesis and Conclusions -- 7. Future Outlook and Perspectives -- References -- Chapter 9. Ocean Circulation/Mixing Studies with Decay-Series Isotopes -- 1. Introduction -- 2. General Transport Equations -- 3. Basic Ocean Mixing/Circulation Models -- 4. Radium Isotopes for Tracing Oceanic Mixing/Circulation -- 5. Radon-222 as a Vertical Mixing Tracer in the Deep Sea -- 6. Actinium-227 as a Diapycnal Mixing Tracer in the Deep Sea -- 7. Tracing Ocean Circulation Using Particle-Reactive Radionuclides -- 8. Closing Remarks and Future Prospects -- Acknowledgments -- References -- Chapter 10. Uranium- and Thorium-Series Radionuclides in Marine Groundwaters -- 1. Introduction. , 2. U- and Th-Series Radionuclides in High-Temperature Marine Groundwaters: Hydrothermal Fluids -- 3. U- and Th-Series Radionuclides in Low-Temperature Marine Groundwaters: Sediment Pore Water -- 4. Future Directions -- Acknowledgments -- References -- Chapter 11. Sediment Signatures of U- and Th-Series Nuclides and their Application as Paleoceanographic Tracers -- 1. Introduction -- 2. Long-Lived U-Series Nuclides in Sediments -- 3. Short-Lived U-Series Nuclides in Sediments: Application to Sediment Mixing and Accumulation -- 4. Authigenic Uranium as a Tracer of Sediment Redox State -- 5. Use of 230Th as a Constant Flux Proxy -- 6. 231Pa/230Th: Proxy for Particle Flux and Productivity -- 7. 231Pa/230Th: Proxy of Ocean Circulation -- 8. Modeling Studies -- 9. Manganese Crusts and Nodules -- 10. Summary and Outlook -- Acknowledgments -- References -- Appendix A. Charts of the 238U, 235U, 232Th, and 241Am Decay Series with Principal Modes of Decay, their Intensities and Energies -- 1. Introduction -- 2. Sources of Data -- References -- Appendix B. Systematics of Radioactive Decay -- 1. Overview of Decay Equations -- 2. Examples of Applications -- References -- Author Index -- Subject Index.
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  • 2
    Buch
    Buch
    Amsterdam : Elsevier
    Schlagwort(e): Uranium-thorium dating ; Water chemistry ; Hydrogeologie ; Grundwasser ; Thorium ; Uran ; Grundwasserstrom ; Tracer ; Meereskunde ; Thorium ; Uran ; Radionuklid ; Hydrogeochemie ; Biogeochemie ; Paläoozeanographie ; Methode ; Anwendung ; Hydrogeologie ; Grundwasser ; Thorium ; Uran ; Grundwasserstrom ; Tracer ; Meereskunde ; Radionuklid ; Hydrogeochemie ; Biogeochemie ; Paläoozeanographie ; Methode ; Anwendung
    Materialart: Buch
    Seiten: XII, 458 S. , Ill., graph. Darst., Kt.
    Ausgabe: 1. ed.
    ISBN: 0080452124 , 9780080450124 , 0080450121
    Serie: Radioactivity in the environment vol. 13
    Sprache: Englisch
    Anmerkung: Includes bibliographical references and index
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  • 3
    Buch
    Buch
    Kidlington : Elsevier Science
    Materialart: Buch
    Seiten: S. 1363 - 1567 , Ill., graph. Darst
    Serie: Deep sea research 56.2009,18
    Sprache: Englisch
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  • 4
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Turekian, Karl K; Cochran, J Kirk; Krishnaswami, Seth; Lanford, W A; Parker, P D; Bauer, K A (1979): The measurement of 10Be in manganese nodules using a tandem Van De Graaff accelerator. Geophysical Research Letters, 6(5), 417-420, https://doi.org/10.1029/GL006i005p00417
    Publikationsdatum: 2023-08-28
    Beschreibung: The growth rate of a manganese nodule from the South Atlantic Ocean (Rio Grande Ridge) has been determined using a 10Be profile as measured with a Tandem Van de Graaff accelerator. This rate is 4.5 mm /My. A correlation may exist between the 10Be flux and the Mn flux to nodules.
    Schlagwort(e): Atlantic Ocean; Beryllium-10; Beryllium-10/Beryllium-9, standard deviation; Beryllium-10/Beryllium-9 ratio; Beryllium-10 decay; Deposit type; DEPTH, sediment/rock; Description; DISTANCE; Distance, maximum; Distance, minimum; Dredge; DRG; Identification; Mass, netto; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; RC16; RC16-10RD; Robert Conrad
    Materialart: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 5
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Krishnaswami, Seth; Cochran, J Kirk (1978): Uranium and thorium series nuclides in oriented ferromanganese nodules: growth rates, turnover times and nuclide behavior. Earth and Planetary Science Letters, 40(1), 45-62, https://doi.org/10.1016/0012-821X(78)90073-0
    Publikationsdatum: 2023-08-28
    Beschreibung: Three ferromanganese nodules handpicked from the tops of 2500 cm**2 area box cores taken from the north equatorial Pacific have been analysed for their U-Th series nuclides. 230Thexc concentrations in the surface 1-2 mm of the top side of the nodules indicate growth rates of 1.8-4.6 mm/10**6 yr. In two of the nodules a significant discontinuity in the 230Th exc depth profile has been observed at ~0.3 m.y. ago, suggesting that the nodule growth has been episodic. The concentration profiles of 231Pa exc (measured via 227Th) yield growth rates similar to the 230Th exc data. The bottom sides of the nodules display exponential decrease of 230Th exc/232Th activity ratio with depth, yielding growth rates of 1.5-3.3 mm/10**6 yr. The 230Th exc and 231Pa exc concentrations in the outermost layer of the bottom face are significantly lower than in the outermost layer of the top face. Comparison of the extrapolated 230Thexc/232Th and 230Th exc/231Pa exc activity ratios for the top and bottom surfaces yields an "age" of (5-15) x 10**4 yr for the bottom relative to the top. This "age" most probably represents the time elapsed since the nodules have attained the present orientation. The 210Pb concentration in the surface ~0.1 mm of the top side is in large excess over its parent 226Ra. Elsewhere in the nodule, up to ~1 mm depth in both top and bottom sides, 210Pb is deficient relative to 226Ra, probably due to 222Rn loss. The absence of 210Pbexc below the outermost layer of the top face rules out the possibility of a sampling artifact as the cause of the observed exponentially decreasing 230Thexc and 231Paexc concentration profiles. The flux of 210Pbexc to the nodules ranges between 0.31 and 0.58 dpm/cm**2/yr. The exhalation rate of 222Rn, estimated from the 226Ra-210Pb disequilibrium is ~570 dpm/cm**2/yr from the top side and 〉2000 dpm/cm**2/yr from the bottom side. 226Ra is deficient in the top side relative to 230Th up to ~0.5-1 mm and is in large excess throughout the bottom. The data indicate a net gain of 226Ra into the nodule, corresponding to a flux of (24-46) x 10**-3 dpm/cm**2/yr. On a total area basis the gain of 226Ra into the nodules is 〈20% of the 226Ra escaping from the sediments. A similar gain of 228Ra into the bottom side of the nodules is reflected by the high 228Th/232Th activity ratios observed in the outermost layer in contact with sediments.
    Schlagwort(e): Alpha counting; BC; Box corer; Deposit type; DEPTH, sediment/rock; Description; DISTANCE; Distance, maximum; Distance, minimum; DOMES-A47-16; DOMES Site C, Pacific Ocean; Elevation of event; Event label; Insoluble residue; Latitude of event; Lead-210; Lead-210, standard deviation; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Pacific Ocean; Radium-226; Radium-226, standard deviation; RP8OC75; RP-8-OC-75; RP8OC7503; RP8OC75-47-16; RP8OC75-57-58; Sample ID; Thorium-227; Thorium-227, standard deviation; Thorium-230; Thorium-230, standard deviation; Thorium-232; Thorium-232, standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 540 data points
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  • 6
    Publikationsdatum: 2022-05-25
    Beschreibung: Author Posting. © The Authors, 2006. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Marine Chemistry 100 (2006): 213-233, doi:10.1016/j.marchem.2005.10.013.
    Beschreibung: Thorium-234 is increasingly used as a tracer of ocean particle flux, primarily as a means to estimate particulate organic carbon export from the surface ocean. This requires determination of both the 234Th activity distribution (in order to calculate 234Th fluxes) and an estimate of the C/234Th ratio on sinking particles, to empirically derive C fluxes. In reviewing C/234Th variability, results obtained using a single sampling method show the most predictable behavior. For example, in most studies that employ in situ pumps to collect size fractionated particles, C/234Th either increases or is relatively invariant with increasing particle size (size classes 〉1 to 100’s μm). Observations also suggest that C/234Th decreases with depth and can vary significantly between regions (highest in blooms of large diatoms and highly productive coastal settings). Comparisons of C fluxes derived from 234Th show good agreement with independent estimates of C flux, including mass balances of C and nutrients over appropriate space and time scales (within factors of 2-3). We recommend sampling for C/234Th from a standard depth of 100 m, or at least one depth below the mixed layer using either large volume size fractionated filtration to capture the rarer large particles, or a sediment trap or other device to collect sinking particles. We also recommend collection of multiple 234Th profiles and C/234Th samples during the course of longer observation periods to better sample temporal variations in both 234Th flux and the characteristic of sinking particles. We are encouraged by new technologies which are optimized to more reliably sample truly settling particles, and expect the utility of this tracer to increase, not just for upper ocean C fluxes but for other elements and processes deeper in the water column.
    Beschreibung: Individuals and science efforts discussed herein were supported by many national science programs, including the U.S. National Science Foundation and U.S. Department of Energy. S.F. and J.C.M. acknowledge the support provided to the International Atomic Energy Agency (IAEA) Marine Environment Laboratory by the Government of the Principality of Monaco. T.T. acknowledges support from the Australian Antarctic Science Program. K.B. was supported in part by a WHOI Ocean Life Institute Fellowship.
    Repository-Name: Woods Hole Open Access Server
    Materialart: Preprint
    Format: 640962 bytes
    Format: application/pdf
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  • 7
    Publikationsdatum: 2022-05-25
    Beschreibung: Author Posting. © The Authors, 2005. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Marine Chemistry 100 (2006): 234-249, doi:10.1016/j.marchem.2005.10.014.
    Beschreibung: Over the past few decades, the radioisotope pair of 238U/234Th has been widely and increasingly used to describe particle dynamics and particle export fluxes in a variety of aquatic systems. The present paper is one of five review articles dedicated to 234Th. It is focused on the models associated with 234Th whereas the companion papers (same issue) are focused on present and future methodologies and techniques (Rutgers van der Loeff et al.), C/234Th ratios (Buesseler et al.), 234Th speciation (Santschi et al.) and present and future applications of 234Th (Waples et al.). In this paper, we review current 234Th scavenging models and discuss the relative importance of the non steady state and physical terms associated with the most commonly used model to estimate 234Th flux. Based on this discussion we recommend that for future work the use of models should be accompanied by a discussion of the effect that model and data uncertainty have on the model results. We also suggest that future field work incorporate repeat occupations of sample sites on time scales of 1-4 weeks in order to evaluate steady state versus non steady state estimates of 234Th export, especially during high flux events (〉 ca. 800 dpm m-2 d-1). Finally, knowledge of the physical oceanography of the study area is essential, particularly in ocean margins and in areas of established upwelling (e.g. Equatorial Pacific). These suggestions will greatly enhance the application of 234Th as a tracer of particle dynamics and flux in more complicated regimes.
    Beschreibung: This paper grew out of discussion held at the “Future Applications of 234Th in Aquatic Systems” workshop held at Woods Hole Oceanographic Institution in August, 2004 (see: http://www.geol.sc.edu/cbnelson/Thmeeting/). We are grateful to the US National Science Foundation Chemical Oceanography Program (OCE 0354757) for its support of the workshop. We thank the US National Science Foundation, the National Oceanic and Atmospheric Administration and the Belgian Science Policy for their support of many of the field and modeling efforts described in this paper.
    Schlagwort(e): Th-234 ; Model ; Scavenging ; Export ; Particle dynamics
    Repository-Name: Woods Hole Open Access Server
    Materialart: Preprint
    Format: 2096326 bytes
    Format: application/pdf
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  • 8
    Digitale Medien
    Digitale Medien
    [s.l.] : Nature Publishing Group
    Nature 280 (1979), S. 385-387 
    ISSN: 1476-4687
    Quelle: Nature Archives 1869 - 2009
    Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik
    Notizen: [Auszug] A 22 cm long valve of an articulated but dead specimen of a vesicomyid clam from the active thermal spring area, called Clambake I1, at a depth of about 2,500 m, was analysed for the radionuclides listed in Table 1 within 1 yr after collection. The valve was cut in half from the hinge to the ...
    Materialart: Digitale Medien
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  • 9
    Publikationsdatum: 2018-03-09
    Beschreibung: A mass balance for the naturally-occurring radium isotopes (224Ra, 223Ra, 228Ra, and 226Ra) in Jamaica Bay, NY, was conducted by directly estimating the individual Ra contributions of wastewater discharge, diffusion from fine-grained subtidal sediments, water percolation through marshes, desorption from resuspended particles, and water exchange at the inlet. The mass balance revealed a major unknown source term accounting for 19–71% of the total Ra input, which could only be resolved by invoking a source from submarine groundwater. Shallow (〈 2 m depth) groundwater from permeable sediments in Jamaica Bay was brackish and enriched in Ra relative to surface bay waters by over two orders of magnitude. To balance Ra fluxes, a submarine groundwater input of 0.8 × 109–9.0 × 109 L d− 1 was required. This flux was similar for all four isotopes, with individual estimates varying by less than a factor of 2. Our calculated groundwater flux was 6- to 70-fold higher than the fresh groundwater discharge to the bay estimated by hydrological methods, but closely matched direct flow rates measured with seepage meters. This suggests that a substantial portion of the discharge consisted of recirculated seawater. The magnitude of submarine groundwater discharge varied seasonally, in the order: summer 〉 autumn 〉 spring. Chemical analyses suggest that the recirculated seawater component of submarine groundwater delivers as much dissolved nitrogen to the bay as the fresh groundwater flux.
    Materialart: Article , PeerReviewed
    Format: text
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  • 10
    Publikationsdatum: 2020-03-20
    Beschreibung: The MedFlux project was devised to determine and model relationships between organic matter and mineral ballasts of sinking particulate matter in the ocean. Specifically we investigated the ballast ratio hypothesis, tested various commonly used sampling and modeling techniques, and developed new technologies that would allow better characterization of particle biogeochemistry. Here we describe the rationale for the project, the biogeochemical provenance of the DYFAMED site, the international support structure, and highlights from the papers published here. Additional MedFlux papers can be accessed at the MedFlux web site (http://msrc.sunysb.edu/MedFlux/).
    Materialart: Article , PeerReviewed
    Format: text
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